Georges Cuvier (1769-1832), one of the founding figures of vertebrate palaeontology, pursued a successful scientific career despite the political upheavals in France during his lifetime. In the 1790s, Cuvier's work on fossils of large mammals including mammoths enabled him to show that extinction was a scientific fact. In 1812 Cuvier published this four-volume illustrated collection of his papers on palaeontology, osteology and stratigraphy. It was followed in 1817 by his famous Le regne animal, available in the Cambridge Library Collection both in French and in Edward Griffith's expanded English translation (1827-35). Volume 2 of Recherches sur les ossemens fossiles describes eleven species of pachyderm found in recent alluvial deposits. They include elephants, mastodons, rhinoceros, hippopotamus, tapir and the hyrax (which Cuvier classified as an ungulate rather than a rodent). Cuvier argued from osteological comparisons with living species that all should be considered distinct species in their own right.

This book gathers and updates the most significant advances of the last two centuries and presents an unprecedented micro paleontological study covering more than 20 stratigraphic sections. This information is supplemented by numerous sedimentological observations and analyses, on the basis of which a new lithostratigraphic framework for the Neogene of the Chacoparanense Basin is proposed. The book is structured in an easy-to-read format: Its main section offers a comprehensive review of the current state of knowledge on transgressions in Argentina and similar transgressions in other South American countries, taking into account various key aspects (age, paleoenvironment, micropaleontology, etc.). Secondly, the book presents the main results on the TLP and TEP of the Chacoparanense Basin and the TEP of the Peninsula de Valdes. Lastly, it provides readers with complete stratigraphic profiles (Appendix A), mineralogical analyses (Appendix B), distribution charts (Appendix C), systematics (Appendix D) and plates (Appendix E).

Georges Cuvier (1769-1832), one of the founding figures of vertebrate palaeontology, pursued a successful scientific career despite the political upheavals in France during his lifetime. In the 1790s, Cuvier's work on fossils of large mammals including mammoths enabled him to show that extinction was a scientific fact. In 1812 Cuvier published this collection of his geological and osteological papers, focusing on living and extinct pachyderms, ruminants, horses and pigs. Volume 1 begins with a substantial essay on human origins and the formation of the earth, which was translated into English by Robert Kerr in 1813 (also available). It also includes an essay on the Egyptian ibis mummy brought back from Napoleon's campaign in Egypt, and an updated version of Cuvier's influential 1810 geological description of the Paris basin, co-authored with Alexandre Brogniart (1770-1847), which helped establish the principle of faunal succession in rock strata of different ages.

For the physician and natural historian John Woodward (c.1655-1728), fossils were the key to unlocking the mystery of the Earth's past, which he attempted to do in this controversial work, first published in 1695 and here reissued in the 1723 third edition. Woodward argues that the 'whole Terrestrial Globe was taken all to Pieces, and dissolved at the Deluge', and that fossilised remains were proof of the flood as described in the Bible. In the first part of the work, Woodward examines other theories of the Earth's history before presenting evidence - much of it based on his own fossil collection - in support of his theory. The work immediately prompted heated debate among his scientific contemporaries. Despite the controversy, Woodward was acknowledged as an expert on fossil classification, cementing this reputation with his influential Fossils of All Kinds (1728), which is also reissued in the Cambridge Library Collection.

The Late Cenozoic Yushe Basin, Shanxi Province, China embodies the bulk of our knowledge on successions of terrestrial vertebrates in the northern part of East Asia. Everything we know about Asian mammals of the last 6 million years has a historical basis in the documentation of the geology of Yushe. This volume introduces the basin in its geological setting, describes the succession of fossiliferous strata, and shows how it is dated. It develops an unsurpassed level of precision for its age control. Geological maps and stratigraphic sections provide the backbone for individual studies to follow on varied fossil groups. The volume explores the history of exploration of the last century in Yushe Basin and places development of paleontology there into the context of the birth of the modern epoch of science in China.

This book serves as an introduction to the Cretaceous geology and palaeontology of south-central Africa, covering the whole of Southern and Eastern Africa and Angola. Fifty two plates illustrate almost 1000 species and provide a field guide to the macrofossils of the subcontinent. The book will be of value to field geologists, students and non-specialists with an interest in the natural world. A bibliography of the Cretaceous palaeontology and stratigraphy of the subcontinent is provided. Features: Provides a concise account of the Cretaceous geology for 13 African regions Includes beautiful illustrations and a comprehensive bibliography Fossils are presented in stratigraphical order, allowing easy determination of the age deposits.

Carbonate sediments are of increasing relevance for archives of past environmental conditions and for economical reasons in areas of geothermal energy and hydrocarbon reservoirs. Complex interaction of physical and chemical parameters with biological parameters determines the architecture and composition of carbonate sedimentary bodies. This book closes some of the still existing gaps in our understanding of the influence and interplay of physical, chemical, and biological parameters with carbonate sedimentation. An understanding of this interaction is not only required for reliable prediction of reservoir quality but also for a robust interpretation of environmental conditions in the past and the present. It is written by geologists for geologists in order to provide an easily accessible overview of the large amount of relevant information provided by the neighbouring sciences. The approach of the book is to document the modern depositional environments of three classical areas of carbonate deposition, each characteristic for a specific sedimentological setting (isolated platform, attached shelf, ramp) in order to assess both the range of physical, biological and chemical parameters and their sedimentary response. This book presents a comprehensive compilation based on data from published work and unpublished theses, and the integration of these data in order to extract previously undiscovered relationships between the discussed parameters and carbonate deposition.

On this blue planet, long before pterodactyls took to the skies and tyrannosaurs prowled the continents, tiny green organisms populated the ancient oceans. Fossil and phylogenetic evidence suggests that chlorophyll, the green pigment responsible for coloring these organisms, has been in existence for some 85% of Earth's long history--that is, for roughly 3.5 billion years. In "How the Earth Turned Green, "Joseph E. Armstrong traces the history of these verdant organisms, which many would call plants, from their ancient beginnings to the diversity of green life that inhabits the Earth today.
Using an evolutionary framework, "How the Earth Turned Green" addresses questions such as: Should all green organisms be considered plants? Why do these organisms look the way they do? How are they related to one another and to other chlorophyll-free organisms? How do they reproduce? How have they changed and diversified over time? And how has the presence of green organisms changed the Earth's ecosystems? More engaging than a traditional textbook and displaying an astonishing breadth, "How the Earth Turned Green" will both delight and enlighten embryonic botanists and any student interested in the evolutionary history of plants.

Barthelemy Faujas de Saint-Fond (1741 1819) abandoned the legal profession to pursue studies in natural history. Appointed a royal commissioner of mines in 1785, he also served as professor of geology at the natural history museum in Paris from 1793 until his death. His keen interest in rocks, minerals and fossils led to a number of important discoveries, among which was confirmation that basalt was a volcanic product. The present work appeared in three parts between 1803 and 1809. The second volume was divided into two. This second part lists the principal active volcanoes around the world and classifies volcanic products. Of related interest in the history of geology, Mineralogie des volcans (1784) and the revised English edition of A Journey through England and Scotland to the Hebrides in 1784 (1907) are two other works by Faujas which are also reissued in this series."

The transition from the Eocene to the Oligocene epochs was the most significant event in earth history since the extinction of dinosaurs. As the first Antarctic ice sheets appeared, major extinctions and faunal turnovers took place on the land and in the sea, eliminating forms adapted to a tropical world and replacing them with the ancestors of most of our modern animal and plant life. Through a detailed study of climatic conditions and of organisms buried in Eocene-Oligocene sediments, this volume shows that the separation of Antarctica from Australia was a critical factor in changing oceanic circulation and ultimately world climate. In this book forty-eight leading scientists examine the full range of Eocene and Oligocene phenomena. Their articles cover nearly every major group of organisms in the ocean and on land and include evidence from paleontology, stable isotopes, sedimentology, seismology, and computer climatic modeling. The volume concludes with an update of the geochronologic framework of the late Paleogene.

Originally published in 1992.

The Princeton Legacy Library uses the latest print-on-demand technology to again make available previously out-of-print books from the distinguished backlist of Princeton University Press. These paperback editions preserve the original texts of these important books while presenting them in durable paperback editions. The goal of the Princeton Legacy Library is to vastly increase access to the rich scholarly heritage found in the thousands of books published by Princeton University Press since its founding in 1905.

This book provides a summary of the discoveries made during the course of excavations at the Paleolithic cave site of Fontechevade, France, between 1994 and 1998. The excavation team used modern field and analytic methods to address major problems raised by earlier excavations at the site from 1937 to 1954. These earlier excavations produced two sets of data that have been problematic in light of data from other European Paleolithic sites: first, the Lower Paleolithic stone tool industry, the Tayacian, that differs in fundamental ways from other contemporary industries and, second, the human skull fragment that has been interpreted as modern in nature but that apparently dates from the last interglacial, long before there is any evidence for humans from any other site in Europe. By applying modern stratigraphic, lithic, faunal, geological, geophysical, and radiometric analyses, the interdisciplinary team demonstrates that the Tayacian industry is a product of site formation processes and that the actual age of the Fontechevade I fossil is compatible with other evidence for the arrival of modern humans in Europe."

Employed early on in his career by Sir Joseph Banks, the botanist John Lindley (1799 1865) went on to conduct important research on the orchid family and also recommended that Kew Gardens should become a national botanical institution. This pioneering three-volume work of palaeobotany, first published between 1831 and 1837, catalogues almost 300 species of fossil plants from the Pleistocene to the Carboniferous period. The geologist and palaeontologist William Hutton (1797 1860), with whom Lindley collaborated, was responsible for collecting the fossil specimens from which the 230 plates were drawn. The first serious attempt at organising and interpreting the evidence of Britain's primeval plant life, this resource is notable also for its prefatory discussion of topics such as coal seams and prehistoric climate. Volume 1 opens with a context-setting introduction and list of genera, followed by the descriptions of plates 1-79."

Originally published in 1921, this book presents a detailed account 'of the two Devonian land floras'. Illustrative figures and textual notes are incorporated throughout. This book will be of value to anyone with an interest in the Devonian period, botany and the history of science.

To the naturalist John Woodward (c.1665 1728), fossils were 'much neglected, and left wholly to the Care and Treatment of Miners and meer Mechanicks'. He had built up a large personal collection of these samples of the Earth's petrified remains and spent much of his life developing a system for their classification, the results of which were published in this important illustrated work of 1728. A distinguished physician and a fellow of the Royal Society, Woodward wrote extensively on scientific topics, and had developed a theory that fossils were creatures destroyed in the flood described in the Bible. These ideas attracted critics and supporters in equal measure, but his contribution to techniques of fossil collection and classification were influential. In the present work, he devotes the early chapters to questions of description and classification, while the later sections contain some of his letters to his scientific contemporaries, including Isaac Newton."

In a one-stop resource, this book provides a state-of-the-art overview of all aspects of pure and applied forams studies. Building from introductory chapters on the history of foraminiferal research, and research methods, the book then takes the reader through biology, ecology, palaeoecology, biostratigraphy and sequence stratigraphy. This is followed by key chapters detailing practical applications of forams in petroleum geology, mineral geology, engineering geology, environmental science and archaeology. All applications are fully supported by numerous case studies selected from around the world, providing a wealth of real-world data. The book also combines lavish illustrations, including over seventy stunning original picture-diagrams of foraminifera, with comprehensive references for further reading, and online data tables providing additional information on hundreds of foram families and species. Accessible and practical, this is a vital resource for graduate students, academic micropalaeontologists and professionals across all disciplines and industry settings which make use of foram studies.

Louis Figuier (1819-94) was destined to remain in academia until disagreements with fellow scholars led him to abandon this path and instead pursue 'the idea that scientific knowledge, which until then had been almost exclusively the property of the learned, should be put within the reach of the reading public'. Published in 1863, La Terre avant le deluge became a classic of popular science and introduced palaeontology to a wider readership; that this English translation appeared only two years later is an indication of its impact. Figuier wrote that his aim was 'to trace the progressive steps by which the earth has reached its present state ... and to describe the various convulsions and transformations through which it has successively passed'. The book was also celebrated for its inclusion of more than 200 illustrations by a pupil of Dore, Edouard Riou (1833-1900), who became famous as Jules Verne's illustrator a few years later.

Employed early on in his career by Sir Joseph Banks, the botanist John Lindley (1799 1865) went on to conduct important research on the orchid family and also recommended that Kew Gardens should become a national botanical institution. This pioneering three-volume work of palaeobotany, first published between 1831 and 1837, catalogues almost 300 species of fossil plants from the Pleistocene to the Carboniferous period. The geologist and palaeontologist William Hutton (1797 1860), with whom Lindley collaborated, was responsible for collecting the fossil specimens from which the 230 plates were drawn. The first serious attempt at organising and interpreting the evidence of Britain's primeval plant life, this resource is notable also for its prefatory discussion of topics such as coal seams and prehistoric climate. Volume 3 includes a note on the action of water on plants. This is followed by the descriptions of plates 157 230."

Employed early on in his career by Sir Joseph Banks, the botanist John Lindley (1799 1865) went on to conduct important research on the orchid family and also recommended that Kew Gardens should become a national botanical institution. This pioneering three-volume work of palaeobotany, first published between 1831 and 1837, catalogues almost 300 species of fossil plants from the Pleistocene to the Carboniferous period. The geologist and palaeontologist William Hutton (1797 1860), with whom Lindley collaborated, was responsible for collecting the fossil specimens from which the 230 plates were drawn. The first serious attempt at organising and interpreting the evidence of Britain's primeval plant life, this resource is notable also for its prefatory discussion of topics such as coal seams and prehistoric climate. Volume 2 opens with a preface on coal, followed by descriptions of some of the fossil plants found therein (plates 80-156)."

Multispecies Archaeology explores the issue of ecological and cultural novelty in the archaeological record from a multispecies perspective. Human exceptionalism and our place in nature have long been topics of academic consideration and archaeology has been synonymous with an axclusively human past, to the detriment of gaining a more nuanced understanding of one that is shared. Encompassing more than just our relationships with animals, the book considers what we can learn about the human past without humans as the focus of the question. The volume digs deep into our understanding of interaction with plants, fungi, microbes, and even the fundamental building blocks of life, DNA. Multispecies Archaeology examines what it means to be human-and non-human-from a variety of perspectives, providing a new lens through which to view the past. Challenging not only the subject or object of archaeology but also broader disciplinary identities, the volume is a landmark in this new and evolving area of scholarly interest.

ANOXIA defines the lack of free molecular oxygen in an environment. In the presence of organic matter, anaerobic prokaryotes produce compounds such as free radicals, hydrogen sulfide, or methane that are typically toxic to aerobes. The concomitance of suppressed respiration and presence of toxic substances suggests these habitats are inhospitable to Eukaryota. Ecologists sometimes term such environments 'Death Zones'. This book presents, however, a collection of remarkable adaptations to anoxia, observed in Eukaryotes such as protists, animals, plants and fungi. Case studies provide evidence for controlled beneficial use of anoxia by, for example, modification of free radicals, use of alternative electron donors for anaerobic metabolic pathways, and employment of anaerobic symbionts. The complex, interwoven existence of oxic and anoxic conditions in space and time is also highlighted as is the idea that eukaryotic inhabitation of anoxic habitats was established early in Earth history.

The invasion of land by ocean-dwelling plants and animals was one of the most revolutionary events in the evolution of life on Earth, yet the animal invasion almost failed-twice-because of the twin mass extinctions of the Late Devonian Epoch. Some 359 to 375 million years ago, these catastrophic events dealt our ancestors a blow that almost drove them back into the sea. If those extinctions had been just a bit more severe, spiders and insects-instead of vertebrates-might have become the ecologically dominant forms of animal life on land. This book examines the profound evolutionary consequences of the Late Devonian extinctions and the various theories proposed to explain their occurrence. Only one group of four-limbed vertebrates exists on Earth, while other tetrapod-like fishes are extinct. This gap is why the idea of "fish with feet" seems so peculiar to us, yet such animals were once a vital part of our world, and if the Devonian extinctions had not happened, members of these species, like the famous Acanthostega and Ichthyostega, might have continued to live in our rivers and lakes. Synthesizing decades of research and including a wealth of new discoveries, this accessible, comprehensive text explores the causes of the Devonian extinctions, the reasons vertebrates were so severely affected, and the potential evolution of the modern world if the extinctions had never taken place.

We cannot catechise our stony ichthyolites, as did the necromantic lady of the Arabian Nights did the coloured fishes of the lake which had once been a city, when she touched their dead bodies with her wand, and they straightaway raised their heads and rephed to her queries. We would have many a question to ask them if we could - questions never to be solved. Hugh Miller, The Old Red Sandstone When I started this book in 1991, the subject of vertebrate origins was fusty and unfashionable. Early drafts for this preface read like an extend ed complaint at the lot of traditional morphologists, cast aside by the march of modern molecular biology. But no longer - this book should reach you at a time of renewed inter est in the origin of the vertebrates, our own particular corner of creation. For although the topic has excited interest for well over a century, molec ular biology has only lately achieved the maturity necessary to test its predictions. As a legitimate field of study, it is fashionable again."

The climate of the Earth has undergone many changes and for those times when geologic data are widespread and abundant the Mesozoic appears to have been one of the warmest intervals. This was a time during which the single continent Pangea disintegrated into continental units similar to those of today, a time when there were no significant polar ice caps and sea level was generally much higher than at the present time, and a time when dinosaurs apparently dominated terrestrial faunas and the flowering plants evolved. Understanding this alien world, ancestral to ours, is intrinsically interesting, intellectually challenging, and offers opportunities for more effective targeting of sites where commercially important geological resources may be found. It also provides critical insights into the operation of coupled Earth systems (biospheric, atmospheric, hydrospheric and geospheric) under extreme 'greenhouse' conditions, and therefore may have relevance to possible future global change. Our intention in organizing this Discussion Meeting was to bring together those who gather and interpret geologic data with those who model global climates from first principles. The community of workers who study the Quaternary have made significant advances by integrating and comparing palaeodata and climate model experiments. Although we have focused not on the Quaternary 'icehouse' but on the Mesozoic 'hothouse' climate we are well aware that approaches used in the study of the Quaternary may have relevance to earlier times.

The culmination of more than a decade of fieldwork and related study, this unique book uses analyses of perimortem taphonomy in Ice Age Siberia to propose a new hypothesis for the peopling of the New World. The authors present evidence based on examinations of more than 9000 pieces of human and carnivore bone from 30 late Pleistocene archaeological and palaeontological sites, including cave and open locations, which span more than 2000 miles from the Ob River in the West to the Sea of Japan in the East. The observed bone damage signatures suggest that the conventional prehistory of Siberia needs revision and, in particular, that cave hyenas had a significant influence on the lives of Ice Age Siberians. The findings are supported by more than 250 photographs, which illustrate the bone damage described and provide a valuable insight into the context and landscape of the fieldwork for those unfamiliar with Siberia.